Australasian monsoon response to Dansgaard-Oeschger event 21 and teleconnections to higher latitudes
Dansgaard-Oeschger (D-O) cycles were the most prominent, abrupt climate events of the last glacial period whose impact was most strongly felt in the high latitudes of the North Atlantic region. The climate links between the North Atlantic, the Asian and A
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|Source:||Earth and Planetary Science Letters|
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